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Magmatism of the submarine Vityaz Ridge (Pacific slope of the Kuril Island Arc)

机译:水下Vityaz山脊(千岛群岛弧的太平洋斜坡)岩浆作用

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摘要

Original results of igneous rock studies are presented. The rocks were dredged during a marine expedition (cruise 37 of R/V Akademik M.A. Lavrent'ev in August-September, 2005) in the region of the submarine Vityaz Ridge and Kuril Arc outer slope. Several age complexes (Late Cretaceous, Eocene, Late Oligocene, Miocene, and Pliocene-Pleistocene) are recognizable on the Vityaz Ridge. These complexes are characterized by a number of common geochemical features since all of them represent the formations of island arc calc-alkali series. At the same time, they also have individual features reflecting different geodynamic settings. The outer slope of the Kuril Arc demonstrates submarine volcanism. The Pliocene-Pleistocene volcanic rocks dredged here are similar to the volcanites of the Kuril-Kamchatka Arc frontal zone. (PUBLICATION ABSTRACT)
机译:提出了火成岩研究的原始结果。这些岩石是在海底Vityaz山脊和千岛弧外坡地区进行的海上探险中挖出的(R / V Akademik M.A. Lavrent'ev巡游37,于2005年进行)。在Vityaz山脊上可以识别出几种年龄的复合体(晚白垩世,始新世,晚渐新世,中新世和上新世-更新世)。这些复合物的特征是具有许多常见的地球化学特征,因为它们都代表了岛弧钙碱系列的形成。同时,它们还具有反映不同地球动力学设置的独特特征。千岛弧的外坡表现出海底火山作用。在这里疏通的上新世至更新世火山岩与千岛—堪察加弧前缘带的火山岩相似。 (出版物摘要)

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